 |
 |
 |
 |
 |
 |
 |
 |
 |
 |
 |
 |
 |
 |
§ |
Solar
Constant (S)
|
|
= solar flux density reaching the
Earth
|
|
= 1370 W/m2
|
|
|
§ |
Solar energy incident on the
Earth
|
|
|
|
= S x
the “flat” area of the Earth
|
|
= S x p R2Earth
|
|
|
§ |
Solar energy absorbed by the
Earth
|
|
=
(received solar flux) – (reflected solar flux)
|
= S p R2Earth – S p R2Earth x
A
|
|
= S p R2Earth x (1-A)
|
|
|
|
A is the planetary
albedo of the Earth, which
|
|
|
is about 0.3.
|
|
|
|